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地质通报  2008 

从同位素年代学发展到构造年代学

, PP. 2014-2015

Keywords: 同位素年代学,热年代学,构造-热年代学,变形年代学,构造年代学

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Abstract:

从同位素年代学发展到构造年代学,中间必需经历热年代学、构?-热年代学和变形年代学等阶段。同位素年代学只是提供简单的地质事件年龄,热年代学使年龄赋予了温度的信息,而构造年代学则强调地质或构造过程时间-空间的四维演化过程。构造年代学使年龄数据的科学意义除了时间,还有温度、地壳深度变化以及流体的是否参与等多重意义,它涉及到多维空间的变化:时间、温度、水平方向的二维变形、垂直方向的变形等。在现有技术和认知水平的条件下,作者强调指出了从变形年代学到构造年代学的发展中要注意的一些关键的问题,而回归传统地质、以野外变形为基础的变形年代学研究是构造年代学发展的前提。

References

[1]  Donson M H. Closure temperature in cooling geochronological and petrological systems[J]. Contrib. Mineral Petrol., 1973, 40: 259-279.
[2]  Harrison T M, Ducan I, McDougall I. Diffusion of ^40Ar in biotitetemperature, pressure and compositional effects[J]. Geochim. Cosmochim., Acta, 1985, 49: 2461-2468.
[3]  Hames W E, Bowring S A. An empirical evaluation of the argon diffusion geometry in muscovite[J]. Earth and Planetary Science Letters, 1994,124: 161-169.
[4]  McDougall I, Harrison T M. Geochronology and thermochronology by the ^40Ar/^39Ar method[M]. New York and Oxford University Press, 1999:1-269.
[5]  American Structural and Tectonics Group. New departures in structural geology and tectonics[M]. 2003,Http://www.pangea.stanford .edu/-dpollard/NSF.
[6]  罗照华 邓晋福.太行山构造岩浆带K―Ar法同位素年龄分析[J].现代地质,:.
[7]  Lovera O M, Richter F M, Harrison T M. The ^40Ar/^39Ar thermochronometry for slowly cooled samples having a distribution of diffusion domain sizes[J]. Journal of Geophysical Research, 1989, 94: 917-935.
[8]  Lee J. Incremental ^40Ar/^39Ar thermochronology of mylonitic rocks from the northern Snake Range, Nevada[J]. Tectonics, 1991,10: 77- 100.
[9]  Ketcham R A, Donelick R A, Donelick M B. AFTSolve: A program for multi-kinetic modeling of apatite fission-track data[J]. Geological Materials Research, 2000, 2(1)(electronic).
[10]  陈文寄 计凤桔 王非.年轻地质体系的年代测定(续)--新方法、新进展[M].北京:地震出版社,1999.90-94.
[11]  陈江峰 刘顺生.大别造山带冷却年龄的^40Ar―^39Ar和裂变径迹年龄测定[J].中国科学:B辑,:.
[12]  Wang G C, Yang W R. Accelerated exhumation during the Cenozoic in the Dabie Mountains: evidence from fission-track ages [J]. Acta Geologica Sinica, 1998,72: 409-419.
[13]  周中毅 潘长春.沉积盆地古地温测定方法及其应用[M].广州:广东科技出版社,1992.
[14]  Forster M A, Lister G S. The interpretation of ^40Ar/^39Ar apparent age spectra produced by mixing: application of the method of asymptotes and limits[J]. Journal of Structural Geology, 2004, 26: 287-305.
[15]  Yang T N, Wang Y, Li J Y, et al. Vertical and horizontal strain partitioning of the central Tianshan (NW China): evidence from structures and ^40Ar/^39Ar geochronology[J]. Journal of Structural Geology, 2007, 29: 1605-1621.
[16]  Wang Y. The onset of the Tan-Lu fault movement in eastern China: constraints from zircon (SHRIMP) and ^40Ar/^39Ar dating[J]. Term Nova, 2006, 18: 423-431.
[17]  Wang Y, Li H M. Initial formation and Mesozoic tectonic exhumation of an intracontinental tectonic belt of the northern part of the Taihang Mountain belt, eastern Asia[J]. Journal of Geology, 2008a, 116:155-172.
[18]  Wang Y, Li J Y, Sun G H. Post-collision eastward extrusion and tectonic exhumation along the eastern Tianshan orogen, central Asia: constraints from dextral strike-slip motion and ^40Ar/^39Ar geochronological evidence[J]. Journal of Geology, 2008b, 116(in press).
[19]  Wang Y, Zhou S. ^40Ar/^39Ar dating constraints on the high-angle normal faulting along the southern segment of the Tan-Lu fault system: An implication for the onset of eastern China rift-systems [J]. Journal of Asian Earth Sciences, 2009,34:51-60.
[20]  Zhu G, Wang Y S, Liu G S, et al. ^40Ar/^39Ar daring of strike-sfip motion on the Tan-Lu fault zone, east China[J]. Journal of Structural Geology, 2005, 27:1379-1398.
[21]  闫全人 胡世玲 等.构造变形/变质作用的精细测年及其在造山带研究中的应用[J].地学前缘,2001,8(3):147-156.
[22]  王勇生 朱光.^40Ar/^39Ar测年中的冷却年龄和变形年龄[J].地质通报,2005,24(3):285-290.
[23]  陈新跃 王岳军 范蔚茗.一种新的构造变形热年代学研究方法--显微构造变形热年代学[J].华东理工学院学报,2006,29:234-238.
[24]  肖庆辉 贾跃明 李晓波 等.中国地质科学近期发展战略的思考[M].武汉:中国地质大学出版社,1991.239-264.
[25]  杨巍然 简平.构造年代学――当今构造研究的一个新学科[J].地质科技情报,:.
[26]  王瑜.构造-热年代学――发展与思考[J].地学前缘,2004,11(4):435-443.

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